Crustal seismic velocity responds to a magmatic intrusion and seasonal loading in Iceland's Northern Volcanic Zone.
Seismic noise interferometry is an exciting technique for studying volcanoes, providing a continuous measurement of seismic velocity changes (dv/v), which are sensitive to magmatic processes that affect the surrounding crust. However, understanding the exact mechanisms causing changes in dv/v is oft...
Main Authors: | , , , |
---|---|
Format: | Text |
Language: | unknown |
Published: |
Apollo - University of Cambridge Repository
2019
|
Subjects: | |
Online Access: | https://dx.doi.org/10.17863/cam.47555 https://www.repository.cam.ac.uk/handle/1810/300483 |